The report, “Policy Implications of Warming Permafrost” released on the sidelines of the UN Climate Change Conference taking place in the Gulf Arab country, said permafrost which covers almost a quarter of the northern hemisphere contains 1,700 gigatonnes of carbon, twice what’s currently in the atmosphere.

“Permafrost is one of the keys to the planet’s future because it contains large stores of frozen organic matter that, if thawed and released into the atmosphere, would amplify current global warming and propel us to a warmer world,” said UN Under-Secretary General and UNEP Executive Director Achim Steiner.

“Its potential impact on the climate, ecosystems and infrastructure has been neglected for too long,” he added. “This report seeks to communicate to climate-treaty negotiators, policy makers and the general public the implications of continuing to ignore the challenges of warming permafrost.”

The report seeks to highlight the potential hazards of carbon dioxide and methane emissions from warming permafrost, which have not thus far been included in climate-prediction modelling. Warming permafrost could emit 43 to 135 gigatonnes of carbon dioxide equivalent by 2100 and 246 to 415 gigatonnes by 2200. Emissions could start within the next few decades and continue for several centuries.

Permafrost emissions could ultimately account for up to 39 per cent of total emissions, and the report’s lead author warned that this must be factored in to the treaty to address global climate change expected to replace the Kyoto Protocol.

“The release of carbon dioxide and methane from warming permafrost is irreversible. Once the organic matter thaws and decays away, there is no way to put it back into the permafrost,” said lead author Kevin Schaefer, from the University of Colorado’s National Snow and Ice Data Center.

“Anthropogenic emissions’ targets in the climate change treaty need to account for these emissions or we risk overshooting the 2°C maximum warming target,” he added.

According to the report, most of the current permafrost formed during or since the last ice age and extends to depths of more than 700 metres in parts of northern Siberia and Canada. Permafrost consists of an active layer of up to two metres in thickness, which thaws each summer and refreezes each winter, and the permanently frozen soil beneath.

Should the active layer increase in thickness due to warming, huge quantities of organic matter stored in the frozen soil would begin to thaw and decay, releasing large amounts of CO₂ and methane into the atmosphere.

Once this process begins, it will operate in a feedback loop known as the permafrost carbon feedback, which has the effect of increasing surface temperatures and thus accelerating the further warming of permafrost—a process that would be irreversible on human timescales.

Arctic and alpine air temperatures are expected to increase at roughly twice the global rate, and climate projections indicate substantial loss of permafrost by 2100. A global temperature increase of 3°C means a 6°C increase in the Arctic, resulting in an irreversible loss of anywhere between 30 to 85 per cent of near-surface permafrost.